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What is Anabatic Wind?

Local winds that blow from slopes to peaks as a result of the heating of the top slopes without being affected by general pressure changes. Generally, the term is used for upward air currents, vertical movements in the formation of cumulus clouds, and valley breezes rather than anabatic winds. Anabatic winds are less common than katabatic winds, which occur through the opposite process.

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Glossary

A line on a weather map connecting points of equal atmospheric pressure, used to identify high and low-pressure systems.

The percentage of water vapor in the air relative to the maximum amount of water vapor the air can hold at a given temperature.

Temperature scale, abbreviated as °C, found by accepting the freezing point of water at one atmospheric pressure as zero...

An instrument that continuously records atmospheric pressure over time. It uses a barometer to measure pressure and creates...

Indicates the amount of water the soil can absorb/retain through percolation. This capacity is around 7% in sandy soil and...

A large body of air having similar horizontal temperature and moisture characteristics.

The amount of water vapor present in the air, which can affect comfort levels and weather conditions.

Jet streams are strong, fast-flowing air currents in the upper levels of the atmosphere. They form when warm air masses meet...

A sudden and rapid flow of snow masses accumulated on the slopes of mountainous areas under the influence of gravity or a...

The trapping of heat in the Earth's atmosphere due to greenhouse gases, such as carbon dioxide and methane, which allows...